Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent

While precipitation over the Tibetan Plateau is a vital resource for glacier mass balance, river runoff and local ecology, the controlling mechanisms are poorly understood. Here, the authors combine observations and simulations and show that convective storms over India sweep moisture up and over th...

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Autores principales:	Wenhao Dong, Yanluan Lin, Jonathon S. Wright, Yi Ming, Yuanyu Xie, Bin Wang, Yong Luo, Wenyu Huang, Jianbin Huang, Lei Wang, Lide Tian, Yiran Peng, Fanghua Xu
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/8012e4602f874fc0a86da4a543c0ce4a
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spelling	oai:doaj.org-article:8012e4602f874fc0a86da4a543c0ce4a2021-12-02T16:57:49ZSummer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent10.1038/ncomms109252041-1723https://doaj.org/article/8012e4602f874fc0a86da4a543c0ce4a2016-03-01T00:00:00Zhttps://doi.org/10.1038/ncomms10925https://doaj.org/toc/2041-1723While precipitation over the Tibetan Plateau is a vital resource for glacier mass balance, river runoff and local ecology, the controlling mechanisms are poorly understood. Here, the authors combine observations and simulations and show that convective storms over India sweep moisture up and over the plateau.Wenhao DongYanluan LinJonathon S. WrightYi MingYuanyu XieBin WangYong LuoWenyu HuangJianbin HuangLei WangLide TianYiran PengFanghua XuNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-9 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Wenhao Dong Yanluan Lin Jonathon S. Wright Yi Ming Yuanyu Xie Bin Wang Yong Luo Wenyu Huang Jianbin Huang Lei Wang Lide Tian Yiran Peng Fanghua Xu Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
description	While precipitation over the Tibetan Plateau is a vital resource for glacier mass balance, river runoff and local ecology, the controlling mechanisms are poorly understood. Here, the authors combine observations and simulations and show that convective storms over India sweep moisture up and over the plateau.
format	article
author	Wenhao Dong Yanluan Lin Jonathon S. Wright Yi Ming Yuanyu Xie Bin Wang Yong Luo Wenyu Huang Jianbin Huang Lei Wang Lide Tian Yiran Peng Fanghua Xu
author_facet	Wenhao Dong Yanluan Lin Jonathon S. Wright Yi Ming Yuanyu Xie Bin Wang Yong Luo Wenyu Huang Jianbin Huang Lei Wang Lide Tian Yiran Peng Fanghua Xu
author_sort	Wenhao Dong
title	Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
title_short	Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
title_full	Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
title_fullStr	Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
title_full_unstemmed	Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent
title_sort	summer rainfall over the southwestern tibetan plateau controlled by deep convection over the indian subcontinent
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/8012e4602f874fc0a86da4a543c0ce4a
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Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent

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